Geological evolution of the Gulf of Saros, NE Aegean Sea

M. N. Çaǧatay; N. Görür; B. Alpar; R. Saatçilar; R. Akkök; M. Sakinç; H. Yüce; C. Yaltirak; I. Kuşcu

doi:10.1007/s003670050045

Geological evolution of the Gulf of Saros, NE Aegean Sea

M. N. Çaǧatay^*, N. Görür, B. Alpar, R. Saatçilar, R. Akkök, M. Sakinç, H. Yüce, C. Yaltirak, I. Kuşcu

^*Corresponding author for this work

Department of Geological Engineering

Research output: Contribution to journal › Article › peer-review

51 Citations (Scopus)

Abstract

The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic régime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.

Original language	English
Pages (from-to)	1-9
Number of pages	9
Journal	Geo-Marine Letters
Volume	18
Issue number	1
DOIs	https://doi.org/10.1007/s003670050045
Publication status	Published - 1998

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10.1007/s003670050045

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abstract = "The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic r{\'e}gime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.",

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T1 - Geological evolution of the Gulf of Saros, NE Aegean Sea

AU - Çaǧatay, M. N.

AU - Görür, N.

AU - Alpar, B.

AU - Saatçilar, R.

AU - Akkök, R.

AU - Sakinç, M.

AU - Yüce, H.

AU - Yaltirak, C.

AU - Kuşcu, I.

PY - 1998

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AB - The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic régime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.

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Geological evolution of the Gulf of Saros, NE Aegean Sea

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